Chapter 12:Agents of Erosion & Deposition Section 3 ... · meltwater. • Streams carry sorted...
Transcript of Chapter 12:Agents of Erosion & Deposition Section 3 ... · meltwater. • Streams carry sorted...
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Chapter 12:Agents of Erosion & Deposition
Section 3: Erosion & Deposition by Ice
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Chapter 12
Glaciers—Rivers of Ice
• A glacier is a large mass of moving ice. They are
capable of eroding, moving, and depositing large
amounts of rock materials.
• Glaciers form in areas so cold that snow stays on
the ground year-round. Because glaciers are so
massive, the pull of gravity causes them to flow
slowly, like “rivers of ice.”
Section 3 Erosion and Deposition by Ice
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Chapter 12
Glaciers—Rivers of Ice, continued
• Alpine Glaciers form in mountainous areas. One
common type of alpine glacier is a valley glacier.
• Valley glaciers form in valleys originally created
by stream erosion. As these glaciers slowly flow
downhill, they widen and straighten the valleys into
broad U shapes.
Section 3 Erosion and Deposition by Ice
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Chapter 12
Glaciers—Rivers of Ice, continued
• Continental Glaciers are huge, continuous masses
of ice that can spread across entire continents.
• The largest continental glacier in the world covers
almost all of Antarctica. This ice sheet is
approximately one and a half times the size of the
United States, and is more than 4,000 m thick in some
places.
Section 3 Erosion and Deposition by Ice
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Chapter 12
• Glaciers on the Move: When enough ice builds
up on a slope, the ice begins to move downhill.
Thick glaciers move faster than thin glaciers, and
the steeper the slope, the faster the glaciers will
move.
• Glaciers move in two ways: sliding and flowing. A
glacier slides when its weight causes the ice at the
bottom to melt. A glacier flows as ice crystals within
the glacier slip over each other.
Section 3 Erosion and Deposition by Ice
Glaciers—Rivers of Ice, continued
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Chapter 12
• Glacier movement is affected by climate. As the
Earth cools, glaciers grow. About 10,000 years
ago, a continental glacier covered most of North
America.
Section 3 Erosion and Deposition by Ice
Glaciers—Rivers of Ice, continued
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Chapter 12
Landforms Carved by Glaciers
• Continental glaciers and alpine glaciers produce
landscapes that are very different from one another.
• Continental glaciers smooth the landscape by
scraping and eroding features that existed before
the ice appeared.
• Alpine glaciers carve out large amounts of rock
material and create spectacular landforms.
Section 3 Erosion and Deposition by Ice
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Chapter 12
Types of Glacial Deposits
• As a glacier melts, it drops all the material it is
carrying. Glacial drift is the general term used to
describe all material carried and deposited by
glaciers.
• Glacial drift is divided into two main types, till
and stratified drift.
Section 3 Erosion and Deposition by Ice
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Chapter 12
Types of Glacial Deposits, continued
• Till Deposits: Unsorted rock material that is
deposited directly by the ice when it melts is called
till. Unsorted means that the till is made up of rock
material of different sizes.
• The most common till deposits are moraines.
Moraines generally form ridges along the edges
of glaciers.
Section 3 Erosion and Deposition by Ice
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Chapter 12
Types of Glacial Deposits, continued • Stratified drift is a glacial deposit that has been
sorted and layered by the action of streams or
meltwater.
• Streams carry sorted material and deposit it in front
of the glacier in a broad area called an outwash
plain.
• Sometimes, a block of ice is left in an outwash plain
when a glacier retreats. As the ice melts, sediment
builds up around the block of ice, forming a
depression called a kettle.
Section 3 Erosion and Deposition by Ice
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